Title: Lecture 11 Evapotranspiration (4)
1Lecture 11 Evapotranspiration (4)
ET Measurements
- Lysimeters
- Evaporation Pans
- Pan size effects
2Lysimeter
- Allow determination of water balance of a block
of soil - Maintain wet soil to measure PET
- Allow soil moisture to fluctuate to measure AET
-
http//lawr.ucdavis.edu/classes/
hyd143/hyd143week2.html
3Weighing Lysimeters
- Use a balance to assess changes in storage
- Small lysimeters can be removed and weighed
- Measure both PET and AET
http//www.kfa-juelich.de/icg/icg5/irapic/einlasse
.jpg
4Draining Lysimeters
- Soil block is isolated but must be undisturbed
and in the same surroundings -
- Cant measure change in storage, only inputs and
outputs
http//www.l-sadwrn.dircon.co.uk/ lysim.html
5Evaporation Pan (US Class A)standard of the
National Weather Service (NWS)
http//www.fao.org/docrep/S2022E/s2022e07.htm
6Sunken Colorado Pan
http//www.fao.org/docrep/S2022E/s2022e07.htm
7Evaporation Pans
Solve a simplified water-balance equation for a
given period (?t)
E W (V2 V1)
E Evaporation W Precipitation during ?t V1
Volume at beginning of ?t V2 Volume at end of
?t
8Estimating the Effect of Pan Size
Empirical equations to account for energy
exchange through the side the pan, in order to
estimate free water evaporation
when Tspan gt Ta - when Tspan lt Ta
Efw Evaporation from free-water surface Epan
Pan evaporation P Atmospheric pressure
(mb) vpan Avg. wind speed 15 cm above pan
(km/day) Tspan Water-surface temperature
(?C) Ta Air temperature (?C) ?pan Proportion
of energy lost to evaporation
Kohler et al. (1955)
9Evaporation Pans
- Free-water evaporation
- Expose a cylindrical (or rectangular) pan of
water to the atmosphere - Provide estimates of potential
evapotranspiration (PET) can be more accurate
than formulae - Must be related to vegetation canopies using
other methods (coefficients etc.) - Precipitation is measured in an adjacent rain
gauge - Pan volume is measured by recording water height
(which is maintained by adding or removing
measured amounts of water) - Pans can be placed on land in clearings or on
floating platforms on open water and usually
surrounded by fences
10Plot Studies
- Water balance approach applied to small
undisturbed plots of land - Analogous to small lake for simple evaporation
- Must select suitable sites where inputs/outputs
can be measured - Spatial uncertainty increases with size of plot
- Artificial rain (sprinklers) can be used to
assess PET - Soil moisture assessed by spot sampling and
measurement by - Gravimetric methods
- Soil block moisture
- Neutron probe
- Time domain reflectometry
11Catchment Studies
- Water balance of entire drainage basin
- Even greater spatial uncertainties
- Variable precipitation, soil water capacity
- Ground water seepage
-
- Better for long term estimates
- On a yearly basis, change in storage is
approx. zero